Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian
Upper Cretaceous strata at Göynük, northwestern Anatolia, Turkey, provide a geological record of the Campanian–Maastrichtian from the Sakarya Terrane along the active Neotethys margin. Shales and shaly marls with siliciclastic and volcaniclastic intercalations indicate a pelagic palaeoenvironment ri...
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Geological Society of London
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ftdatacite:10.6084/m9.figshare.c.4777556.v1 2023-05-15T18:00:21+02:00 Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian Wolfgring, Erik Wagreich, Michael Yilmaz, Ismail O. Shasha, Liu Boehm, Katharina 2019 https://dx.doi.org/10.6084/m9.figshare.c.4777556.v1 https://geolsoc.figshare.com/collections/Late_Cretaceous_stratigraphy_in_the_Mudurnu_G_yn_k_Basin_Turkey_and_inferences_on_sea-level_change_in_the_Late_Campanian_to_Early_Maastrichtian/4777556/1 unknown Geological Society of London https://dx.doi.org/10.1144/sp498-2018-145 https://dx.doi.org/10.6084/m9.figshare.c.4777556 CC BY 4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Geology FOS Earth and related environmental sciences Collection article 2019 ftdatacite https://doi.org/10.6084/m9.figshare.c.4777556.v1 https://doi.org/10.1144/sp498-2018-145 https://doi.org/10.6084/m9.figshare.c.4777556 2021-11-05T12:55:41Z Upper Cretaceous strata at Göynük, northwestern Anatolia, Turkey, provide a geological record of the Campanian–Maastrichtian from the Sakarya Terrane along the active Neotethys margin. Shales and shaly marls with siliciclastic and volcaniclastic intercalations indicate a pelagic palaeoenvironment rich in planktonic and benthonic foraminifera and calcareous nannofossil assemblages. A composite record from the Campanian to the Maastrichtian records nannofossil standard zones UC15c (CC21) to UC20a (CC26) as well as the Globotrunanella havanensis planktonic foraminifera Zone to the Racemiguembelina fructicosa planktonic foraminifera Zone. The complete `mid'-Campanian to early Maastrichtian composite section can be correlated to other western Tethyan sections. The Campanian–Maastrichtian boundary is positioned between the first occurrence of the planktonic foraminifera Gansserina gansseri and the last occurrence of the nannofossil Uniplanarius trifidus . Clastic input and higher sedimentation rates constrain regional sea-level lowstands around the late Campanian calcarata Zone and the Campanian–Maastrichtian boundary, corresponding to the Campanian–Maastrichtian boundary event. Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
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unknown |
topic |
Geology FOS Earth and related environmental sciences |
spellingShingle |
Geology FOS Earth and related environmental sciences Wolfgring, Erik Wagreich, Michael Yilmaz, Ismail O. Shasha, Liu Boehm, Katharina Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
topic_facet |
Geology FOS Earth and related environmental sciences |
description |
Upper Cretaceous strata at Göynük, northwestern Anatolia, Turkey, provide a geological record of the Campanian–Maastrichtian from the Sakarya Terrane along the active Neotethys margin. Shales and shaly marls with siliciclastic and volcaniclastic intercalations indicate a pelagic palaeoenvironment rich in planktonic and benthonic foraminifera and calcareous nannofossil assemblages. A composite record from the Campanian to the Maastrichtian records nannofossil standard zones UC15c (CC21) to UC20a (CC26) as well as the Globotrunanella havanensis planktonic foraminifera Zone to the Racemiguembelina fructicosa planktonic foraminifera Zone. The complete `mid'-Campanian to early Maastrichtian composite section can be correlated to other western Tethyan sections. The Campanian–Maastrichtian boundary is positioned between the first occurrence of the planktonic foraminifera Gansserina gansseri and the last occurrence of the nannofossil Uniplanarius trifidus . Clastic input and higher sedimentation rates constrain regional sea-level lowstands around the late Campanian calcarata Zone and the Campanian–Maastrichtian boundary, corresponding to the Campanian–Maastrichtian boundary event. |
format |
Article in Journal/Newspaper |
author |
Wolfgring, Erik Wagreich, Michael Yilmaz, Ismail O. Shasha, Liu Boehm, Katharina |
author_facet |
Wolfgring, Erik Wagreich, Michael Yilmaz, Ismail O. Shasha, Liu Boehm, Katharina |
author_sort |
Wolfgring, Erik |
title |
Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
title_short |
Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
title_full |
Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
title_fullStr |
Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
title_full_unstemmed |
Late Cretaceous stratigraphy in the Mudurnu–Göynük Basin (Turkey) and inferences on sea-level change in the Late Campanian to Early Maastrichtian |
title_sort |
late cretaceous stratigraphy in the mudurnu–göynük basin (turkey) and inferences on sea-level change in the late campanian to early maastrichtian |
publisher |
Geological Society of London |
publishDate |
2019 |
url |
https://dx.doi.org/10.6084/m9.figshare.c.4777556.v1 https://geolsoc.figshare.com/collections/Late_Cretaceous_stratigraphy_in_the_Mudurnu_G_yn_k_Basin_Turkey_and_inferences_on_sea-level_change_in_the_Late_Campanian_to_Early_Maastrichtian/4777556/1 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1144/sp498-2018-145 https://dx.doi.org/10.6084/m9.figshare.c.4777556 |
op_rights |
CC BY 4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.c.4777556.v1 https://doi.org/10.1144/sp498-2018-145 https://doi.org/10.6084/m9.figshare.c.4777556 |
_version_ |
1766169400094752768 |